High-temperature K2COC14: orthorhombic, a=26.838 (3), b=12.406 (1), c=7.262 (1 )~ , space group Pna21, Z = 1 2 , adopts a slightly modified fl-KzSO4 structure. Low-temperature K2COC14: monoclinic, a=6.801 (1), b=9.569 (1), c=12.757 (1)/~,, ,8=107.0 (1) °, space group P21/c, Z = 4 , adopts a strongly distorted ,8-K2SO4 structure. Introduction. The structure determination of KzCoC14 is part of an investigation of structural relationships and magnetic properties of ternary halides AxByXz with A an alkali metal, B a first-row transition element or an alkaline-earth metal and X = C1, Br or I. The phase diagram of the system KCI-CoCIz was constructed by Seifert (1961). Apart from K2COC14 (m.p. 436°C) it shows another compound, KCoC13, but not the phase transition we observe for K2CoCI 4. By melting stoichiometric amounts of KC1 and CoClz in an evacuated quartz tube and annealing the mixture at 400°C for one week, the orthorhombic modification of KzCoCI4 is obtained. After a few months this phase changes at room temperature into the monoclinic modification. The former is again obtained after annealing the latter at 400°C. The two phases are easily recognized by their X-ray powder diagrams. We were unable to measure the transition temperature by means of DTA, but visual inspection of samples after heating suggests a phase transition between 350 and 360°C. Lamotte & Vermeire (1975) report that powder diffractograms of K2COC14 and (NHa)zZnCI 4 can be indexed on the basis of an orthorhombic cell with axes a=8.90, b=12.39 and c=7.25 (.~) for KzCoCI4 and a=9.20, b = 12.56 and c=7.17 (•) for (NH4)2ZnCI 4. In both cases our diagrams show powder lines between d=3.47 and 3.51 A, which cannot be indexed with these cell parameters. On tripling the a parameter these reflexions can be indexed as 202, 231 and 112. Klug & Sears (1945) also report a tripled a parameter for KzZnCI4, based on single-crystal measurements. Dry KCI was obtained by heating in vacuo at 400 °C, and dry COC12 by heating COC12.6HzO in a stream of dry HCI gas at 400°C. Lowand high-temperature KzCoCI4 were obtained by melting a stoichiometric mixture of KCI and CoCIz in an evacuated sealed quartz tube and slowly lowering the temperature over the course of a few days to room temperature with a temperature gradient of about 50°C, with the higher temperature at the top of the melt. All manipulations of KzCoCI 4 were carried out in a glovebox filled with dry N2 or under dry paraffin oil. The crystallized blue material was broken into pieces and crystals were selected. A series of Weissenberg photographs showed some crystals with orthorhombic and some with monoclinic symmetry. One suitable crystal of each phase was collected and measured by means of an Enraf-Nonius three-circle single-crystal diffractometer. Intensities were recorded by the 0-20 scan method for all reflexions with 0 between 3 and 30 °. Monochromatic (graphite) Mo K0~ radiation was used for measuring the intensities. Background inteni ° sities were determined at 0+~zl , with z1=0.7+1.3 tan 0 °. The mean counting time was 25 s for each background and 50 s for the scan. Standard deviations were calculated from counting statistics. Absorption corrections were applied with a computer program written by de Graaff (1973), and new standard deviations (av) were calculated taking into account the inaccuracy of the absorption correction and attenuation factors of the filters used. Non-equivalent significant reflexions were reduced to F values and Wilson plots were calculated, yielding approximate values for the scale factors and overall isotropic temperature parameters, B. Table 1 gives the crystal and diffraction data. According to the reflexion conditions for orthorhombic KzCoCI4, another space group (Pnam) is possible, which the Patterson synthesis proved to be incorrect. Table 1. Crystal and diffraction data for K2CoCI 4
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